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Geophysical Investigation of a Solid Waste Disposal Site Using Integrated Electrical Resistivity Tomography and Multichannel Analyses of Surface Waves Methods

机译:综合电阻率层析成像和表面波多通道分析法对固体废物处置场进行地球物理研究

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Electrical resistivity tomography survey was deployed at a solid waste landfill in southwest Missouri USA with the intent to map variations in moisture content through the solid waste and underlying subsurface, and to map the top of bedrock. Multichannel analyses of surface waves survey was also deployed to map variations in engineering properties of the solid waste and underlying subsurface, and to constrain the interpretations of top of bedrock. The 2-D resistivity images through the waste suggest rainwater seeps through the cap cover system of the solid waste landfill, and moisture content within the solid waste increases with solid waste burial depth. The resistivity anomalies displayed by the soil and bedrock directly underneath the solid waste suggests a lateral component to moisture infiltrating at the toe of the landfill, which is flowing inward to the base of solid waste structural low. The 1-D shear wave velocity profiles obtained from the multichannel analyses of surface waves survey helped interpret the top of bedrock underneath the solid waste, where top of bedrock is difficult to map using electrical resistivity tomography, as shallow fractured bedrock is moist and displays comparable resistivity values to that of overlying soil. Not surprisingly, the top of bedrock is readily identified on the electrical resistivity tomography profiles in places where subsurface is relatively dry. The deployment of the combined non- invasive, cost and time effective geophysical surveys, along with engineering judgement on available site history data, has reasonably identified potential landfill seepage pathways. The methodology presented could be used in similar site investigation settings.
机译:电阻率断层扫描调查部署在密苏里州西南部的固体废物垃圾填埋场,目的是通过固体废物和底层地下映射水分含量的变化,并映射基岩顶部。表面波的多通道分析还部署到映射固体废物和底层地下的工程性质的变化,并限制基岩顶部的解释。通过废物的2-D电阻率图像显示雨水通过固体废物填埋场的盖盖系统,固体废物内的水分含量随着固体废物埋深深度而增加。土壤和基岩直接在固体废物下方显示的电阻性异常表明侧面部件在垃圾填埋场脚趾处渗透到垃圾填埋场的湿润,这在固体废物结构低的基础上向内流动。从表面波的多通道分析获得的1-D剪切波速度谱有助于解释固体废物下方的基岩顶部,在基岩顶部难以使用电阻率断层扫描来映射,因为浅碎屑是潮湿的,并且显示可比较覆盖土的电阻率值。毫不奇怪,在地下相对干燥的地方的电阻率断层扫描曲线上容易识别基岩顶部。组合非侵入性,成本和时间有效地球物理调查的部署以及对可用现场历史数据的工程判断,具有合理识别潜在的垃圾填埋场渗流途径。呈现的方法可以用于类似的网站调查设置。

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